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T54/55 Variants in detail by Frantisek Koran

By Frantisek Koran

The T-54 and T-55 tanks have been a sequence of major conflict tanks designed within the Soviet Union. the 1st T-54 prototype seemed in March 1945, in advance of the tip of the second one global conflict. The T-54 entered complete creation in 1947 and have become the most tank for armored devices of the Soviet military, armies of the Warsaw Pact nations, and others. T-54s and T-55s have been interested by a number of the worlds armed conflicts throughout the past due 20th century.The T-54/55 sequence finally grew to become the most-produced tank in historical past. anticipated creation numbers for the sequence diversity from 86,000 to 100,000.

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2000) Annular modes in the extratropical circulation, Part II: Trends. J. Clim. 13, 1018–1036. , Sheldon, F. and Crabb, P. (2004) A Hydrological Perspective on the Darling River. In: The Darling (Ed. by R. Breckwoldt, R. Boden and J. Andrew), pp. 332–347. Murray‐Darling Basin Commission, Canberra. L. (1976) Fluctuations and trends in indices of the Southern Hemisphere circulation. Q. J. R. Meteorol. Soc. 102, 65–75. J. ’’ Q. J. R. Meteorol. Soc. 91, 490–506. Vives, B. and Jones, R. 73. CSIRO Marine and Atmospheric Research.

PITTOCK ET AL. further and suggested that the rainfall changes around 1945–1946 might prove to be partly due to global warming and a good analogy of what might be expected in future. The first specific analysis of possible changes in the MDB, with implications for irrigated agriculture, was published by Pigram et al. (1992). This was based on climate change scenarios issued by CSIRO in 1992, but did not discuss floods. Several later studies were undertaken on water resources including parts of the MDB.

And Kuczera, G. (2002) Flood frequency analysis: Evidence and implications of secular climate variability, New South Wales. Water Resour. Res. 38, art. no. 1062. Gentilli, J. (1971) Climatic fluctuation: Climates of Australia and New Zealand. World Surv. Climatol. 13, 89. C. (1988) The rain event of 25–26 January 1984 over the Australian Capital Territory and surrounding districts of New South Wales. Meteorological Note 180, Bureau of Meteorology, Melbourne. M. B. (1997) Changes in daily precipitation under enhanced greenhouse conditions.

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